Emission and flux of DMS from the Australian Antarctic and Subantarctic Oceans during the 1988/89 summer
Identifieur interne : 000841 ( Istex/Corpus ); précédent : 000840; suivant : 000842Emission and flux of DMS from the Australian Antarctic and Subantarctic Oceans during the 1988/89 summer
Auteurs : A. R. Mctaggart ; H. R. Burton ; B. C. NguyenSource :
- Journal of Atmospheric Chemistry [ 0167-7764 ] ; 1995-01-01.
English descriptors
- KwdEn :
- Andreae, Antarctic, Antarctic continent, Antarctic convergence, Antarctic divergence, Antarctic ocean, Austral summer, Australasian, Australasian antarctic, Australasian antarctic ocean, Australasian sector, Divergence, Geophys, January, Mctaggart, Nguyen, November, Offshelf waters, Piston velocity, Schmidt number, Seawater, Southern ocean, Subantarctic, Subantarctic ocean, Subantarctic oceans, Water masses, Wind speed, Wind speeds.
- Teeft :
- Andreae, Antarctic, Antarctic continent, Antarctic convergence, Antarctic divergence, Antarctic ocean, Austral summer, Australasian, Australasian antarctic, Australasian antarctic ocean, Australasian sector, Divergence, Geophys, January, Mctaggart, Nguyen, November, Offshelf waters, Piston velocity, Schmidt number, Seawater, Southern ocean, Subantarctic, Subantarctic ocean, Subantarctic oceans, Water masses, Wind speed, Wind speeds.
Abstract
Abstract: DMS emissions and fluxes from the Australasian sector of the Antarctic and Subantarctic Oceans, bound by 46–68° S and 65.5–142.6° E, were determined from a limited number of samples (n=32) collected during three summer resupply voyages to Australian Antarctic continental research bases between November 1988 and January 1989 (a 92 day period). The maximum DMS emission from this sector of the Antarctic Ocean was in an area near the Antarctic Divergence (60–63° S) and the minimum DMS emission was from the Antarctic coastal and offshelf waters. The greatest emission of DMS from this sector of the Southern Ocean was from the Subantarctic waters. DMS flux from the Australasian Antarctic Ocean was 64.3×106 (±115) mol d−1 or 5.9 (±10.6)×109 mol based on an emission of 10.9 (±19.5) µmol m−2 d−1 (n=26). The flux of DMS from the Australasian sector of the Subantarctic Ocean was probably twice the flux of DMS from the adjacent Antarctic Ocean.
Url:
DOI: 10.1007/BF01099918
Links to Exploration step
ISTEX:2B29DC7FF4A6B364AAAD2B85B2673778594C2E1ELe document en format XML
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The maximum DMS emission from this sector of the Antarctic Ocean was in an area near the Antarctic Divergence (60–63° S) and the minimum DMS emission was from the Antarctic coastal and offshelf waters. The greatest emission of DMS from this sector of the Southern Ocean was from the Subantarctic waters. DMS flux from the Australasian Antarctic Ocean was 64.3×106 (±115) mol d−1 or 5.9 (±10.6)×109 mol based on an emission of 10.9 (±19.5) µmol m−2 d−1 (n=26). 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Nguyen</name><affiliations><json:string>Centre des Faibles Radioactivites, Laboratoire Mixte CNRS, CEA, Avenue de la Terrasse, F-91198, Gif sur Yvette Cedex, France</json:string></affiliations></json:item></author><articleId><json:string>BF01099918</json:string><json:string>Art4</json:string></articleId><arkIstex>ark:/67375/1BB-V549MB0T-P</arkIstex><language><json:string>eng</json:string></language><originalGenre><json:string>OriginalPaper</json:string></originalGenre><abstract>Abstract: DMS emissions and fluxes from the Australasian sector of the Antarctic and Subantarctic Oceans, bound by 46–68° S and 65.5–142.6° E, were determined from a limited number of samples (n=32) collected during three summer resupply voyages to Australian Antarctic continental research bases between November 1988 and January 1989 (a 92 day period). The maximum DMS emission from this sector of the Antarctic Ocean was in an area near the Antarctic Divergence (60–63° S) and the minimum DMS emission was from the Antarctic coastal and offshelf waters. The greatest emission of DMS from this sector of the Southern Ocean was from the Subantarctic waters. DMS flux from the Australasian Antarctic Ocean was 64.3×106 (±115) mol d−1 or 5.9 (±10.6)×109 mol based on an emission of 10.9 (±19.5) µmol m−2 d−1 (n=26). The flux of DMS from the Australasian sector of the Subantarctic Ocean was probably twice the flux of DMS from the adjacent Antarctic Ocean.</abstract><qualityIndicators><score>7.474</score><pdfWordCount>3614</pdfWordCount><pdfCharCount>19056</pdfCharCount><pdfVersion>1.3</pdfVersion><pdfPageCount>11</pdfPageCount><pdfPageSize>461 x 684 pts</pdfPageSize><refBibsNative>false</refBibsNative><abstractWordCount>155</abstractWordCount><abstractCharCount>955</abstractCharCount><keywordCount>0</keywordCount></qualityIndicators><title>Emission and flux of DMS from the Australian Antarctic and Subantarctic Oceans during the 1988/89 summer</title><genre><json:string>research-article</json:string></genre><host><title>Journal of Atmospheric Chemistry</title><language><json:string>unknown</json:string></language><publicationDate>1995</publicationDate><copyrightDate>1995</copyrightDate><issn><json:string>0167-7764</json:string></issn><eissn><json:string>1573-0662</json:string></eissn><journalId><json:string>10874</json:string></journalId><volume>20</volume><issue>1</issue><pages><first>59</first><last>69</last></pages><genre><json:string>journal</json:string></genre><subject><json:item><value>Meteorology/Climatology</value></json:item><json:item><value>Atmospheric Protection/Air Quality Control/Air Pollution</value></json:item></subject></host><namedEntities><unitex><date><json:string>1988</json:string><json:string>between November 1988 and January 1989</json:string><json:string>1993-10-12</json:string><json:string>1989</json:string></date><geogName><json:string>OCEAN Typically</json:string><json:string>region of the Southern Ocean</json:string><json:string>Region of the Antarctic Ocean</json:string><json:string>OCEAN High</json:string></geogName><orgName><json:string>Indiana University</json:string></orgName><orgName_funder></orgName_funder><orgName_provider></orgName_provider><persName><json:string>S. 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The maximum DMS emission from this sector of the Antarctic Ocean was in an area near the Antarctic Divergence (60–63° S) and the minimum DMS emission was from the Antarctic coastal and offshelf waters. The greatest emission of DMS from this sector of the Southern Ocean was from the Subantarctic waters. DMS flux from the Australasian Antarctic Ocean was 64.3×106 (±115) mol d−1 or 5.9 (±10.6)×109 mol based on an emission of 10.9 (±19.5) µmol m−2 d−1 (n=26). The flux of DMS from the Australasian sector of the Subantarctic Ocean was probably twice the flux of DMS from the adjacent Antarctic Ocean.</p></abstract><textClass><keywords scheme="Journal Subject"><list><head>Geosciences</head><item><term>Meteorology/Climatology</term></item><item><term>Atmospheric Protection/Air Quality Control/Air Pollution</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="1993-10-12">Created</change><change when="1995-01-01">Published</change><change xml:id="refBibs-istex" who="#ISTEX-API" when="2017-10-3">References added</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/2B29DC7FF4A6B364AAAD2B85B2673778594C2E1E/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Springer, Publisher found" wicri:toSee="no header"><istex:xmlDeclaration>version="1.0" 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Pollution</JournalSubject></JournalSubjectGroup></JournalInfo><Volume><VolumeInfo VolumeType="Regular" TocLevels="0"><VolumeIDStart>20</VolumeIDStart><VolumeIDEnd>20</VolumeIDEnd><VolumeIssueCount>3</VolumeIssueCount></VolumeInfo><Issue IssueType="Regular"><IssueInfo TocLevels="0"><IssueIDStart>1</IssueIDStart><IssueIDEnd>1</IssueIDEnd><IssueArticleCount>6</IssueArticleCount><IssueHistory><CoverDate><Year>1995</Year><Month>1</Month></CoverDate></IssueHistory><IssueCopyright><CopyrightHolderName>Kluwer Academic Publishers</CopyrightHolderName><CopyrightYear>1995</CopyrightYear></IssueCopyright></IssueInfo><Article ID="Art4"><ArticleInfo Language="En" ArticleType="OriginalPaper" NumberingStyle="Unnumbered" TocLevels="0" ContainsESM="No"><ArticleID>BF01099918</ArticleID><ArticleDOI>10.1007/BF01099918</ArticleDOI><ArticleSequenceNumber>4</ArticleSequenceNumber><ArticleTitle Language="En">Emission and flux of DMS from the Australian Antarctic and Subantarctic Oceans during the 1988/89 summer</ArticleTitle><ArticleFirstPage>59</ArticleFirstPage><ArticleLastPage>69</ArticleLastPage><ArticleHistory><RegistrationDate><Year>2004</Year><Month>11</Month><Day>10</Day></RegistrationDate><Received><Year>1993</Year><Month>10</Month><Day>12</Day></Received><Revised><Year>1994</Year><Month>11</Month><Day>7</Day></Revised></ArticleHistory><ArticleCopyright><CopyrightHolderName>Kluwer Academic Publishers</CopyrightHolderName><CopyrightYear>1995</CopyrightYear></ArticleCopyright><ArticleGrants Type="Regular"><MetadataGrant Grant="OpenAccess"></MetadataGrant><AbstractGrant Grant="OpenAccess"></AbstractGrant><BodyPDFGrant Grant="Restricted"></BodyPDFGrant><BodyHTMLGrant Grant="Restricted"></BodyHTMLGrant><BibliographyGrant Grant="Restricted"></BibliographyGrant><ESMGrant Grant="Restricted"></ESMGrant></ArticleGrants><ArticleContext><JournalID>10874</JournalID><VolumeIDStart>20</VolumeIDStart><VolumeIDEnd>20</VolumeIDEnd><IssueIDStart>1</IssueIDStart><IssueIDEnd>1</IssueIDEnd></ArticleContext></ArticleInfo><ArticleHeader><AuthorGroup><Author AffiliationIDS="Aff1" CorrespondingAffiliationID="Aff2" PresentAffiliationID="Aff2"><AuthorName DisplayOrder="Western"><GivenName>A.</GivenName><GivenName>R.</GivenName><FamilyName>McTaggart</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff1"><AuthorName DisplayOrder="Western"><GivenName>H.</GivenName><GivenName>R.</GivenName><FamilyName>Burton</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff3"><AuthorName DisplayOrder="Western"><GivenName>B.</GivenName><GivenName>C.</GivenName><FamilyName>Nguyen</FamilyName></AuthorName></Author><Affiliation ID="Aff1"><OrgDivision>Australian Antarctic Division</OrgDivision><OrgName>Channel Highway</OrgName><OrgAddress><Postcode>7150</Postcode><City>Kingston</City><State>Tasmania</State><Country>Australia</Country></OrgAddress></Affiliation><Affiliation ID="Aff3"><OrgDivision>Centre des Faibles Radioactivites</OrgDivision><OrgName>Laboratoire Mixte CNRS, CEA</OrgName><OrgAddress><Street>Avenue de la Terrasse</Street><Postcode>F-91198</Postcode><City>Gif sur Yvette Cedex</City><Country>France</Country></OrgAddress></Affiliation><Affiliation ID="Aff2"><OrgDivision>Biogeochemical Laboratories, Geology 307</OrgDivision><OrgName>Indiana University</OrgName><OrgAddress><Postcode>47404-1403</Postcode><City>Bloomington</City><State>IN</State><Country>USA</Country></OrgAddress></Affiliation></AuthorGroup><Abstract ID="Abs1" Language="En"><Heading>Abstract</Heading><Para>DMS emissions and fluxes from the Australasian sector of the Antarctic and Subantarctic Oceans, bound by 46–68° S and 65.5–142.6° E, were determined from a limited number of samples (<Emphasis Type="Italic">n</Emphasis>=32) collected during three summer resupply voyages to Australian Antarctic continental research bases between November 1988 and January 1989 (a 92 day period). The maximum DMS emission from this sector of the Antarctic Ocean was in an area near the Antarctic Divergence (60–63° S) and the minimum DMS emission was from the Antarctic coastal and offshelf waters. The greatest emission of DMS from this sector of the Southern Ocean was from the Subantarctic waters. DMS flux from the Australasian Antarctic Ocean was 64.3×10<Superscript>6</Superscript> (±115) mol d<Superscript>−1</Superscript> or 5.9 (±10.6)×10<Superscript>9</Superscript> mol based on an emission of 10.9 (±19.5) µmol m<Superscript>−2</Superscript> d<Superscript>−1</Superscript> (<Emphasis Type="Italic">n</Emphasis>=26). The flux of DMS from the Australasian sector of the Subantarctic Ocean was probably twice the flux of DMS from the adjacent Antarctic Ocean.</Para></Abstract><KeywordGroup Language="En"><Heading>Key words</Heading><Keyword>DMS</Keyword><Keyword>emission and flux</Keyword><Keyword>Australasian Antarctic and Subantarctic Oceans</Keyword></KeywordGroup></ArticleHeader><NoBody></NoBody></Article></Issue></Volume></Journal></Publisher></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Emission and flux of DMS from the Australian Antarctic and Subantarctic Oceans during the 1988/89 summer</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Emission and flux of DMS from the Australian Antarctic and Subantarctic Oceans during the 1988/89 summer</title></titleInfo><name type="personal" displayLabel="corresp"><namePart type="given">A.</namePart><namePart type="given">R.</namePart><namePart type="family">McTaggart</namePart><affiliation>Australian Antarctic Division, Channel Highway, 7150, Kingston, Tasmania, Australia</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">H.</namePart><namePart type="given">R.</namePart><namePart type="family">Burton</namePart><affiliation>Australian Antarctic Division, Channel Highway, 7150, Kingston, Tasmania, Australia</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">B.</namePart><namePart type="given">C.</namePart><namePart type="family">Nguyen</namePart><affiliation>Centre des Faibles Radioactivites, Laboratoire Mixte CNRS, CEA, Avenue de la Terrasse, F-91198, Gif sur Yvette Cedex, France</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="research-article" displayLabel="OriginalPaper" authority="ISTEX" authorityURI="https://content-type.data.istex.fr" valueURI="https://content-type.data.istex.fr/ark:/67375/XTP-1JC4F85T-7">research-article</genre><originInfo><publisher>Kluwer Academic Publishers</publisher><place><placeTerm type="text">Dordrecht</placeTerm></place><dateCreated encoding="w3cdtf">1993-10-12</dateCreated><dateIssued encoding="w3cdtf">1995-01-01</dateIssued><dateIssued encoding="w3cdtf">1995</dateIssued><copyrightDate encoding="w3cdtf">1995</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><abstract lang="en">Abstract: DMS emissions and fluxes from the Australasian sector of the Antarctic and Subantarctic Oceans, bound by 46–68° S and 65.5–142.6° E, were determined from a limited number of samples (n=32) collected during three summer resupply voyages to Australian Antarctic continental research bases between November 1988 and January 1989 (a 92 day period). The maximum DMS emission from this sector of the Antarctic Ocean was in an area near the Antarctic Divergence (60–63° S) and the minimum DMS emission was from the Antarctic coastal and offshelf waters. The greatest emission of DMS from this sector of the Southern Ocean was from the Subantarctic waters. DMS flux from the Australasian Antarctic Ocean was 64.3×106 (±115) mol d−1 or 5.9 (±10.6)×109 mol based on an emission of 10.9 (±19.5) µmol m−2 d−1 (n=26). The flux of DMS from the Australasian sector of the Subantarctic Ocean was probably twice the flux of DMS from the adjacent Antarctic Ocean.</abstract><relatedItem type="host"><titleInfo><title>Journal of Atmospheric Chemistry</title></titleInfo><titleInfo type="abbreviated"><title>J Atmos Chem</title></titleInfo><genre type="journal" displayLabel="Archive Journal" authority="ISTEX" valueURI="https://publication-type.data.istex.fr/ark:/67375/JMC-0GLKJH51-B">journal</genre><originInfo><publisher>Springer</publisher><dateIssued encoding="w3cdtf">1995-01-01</dateIssued><copyrightDate encoding="w3cdtf">1995</copyrightDate></originInfo><subject><genre>Geosciences</genre><topic>Meteorology/Climatology</topic><topic>Atmospheric Protection/Air Quality Control/Air Pollution</topic></subject><identifier type="ISSN">0167-7764</identifier><identifier type="eISSN">1573-0662</identifier><identifier type="JournalID">10874</identifier><identifier type="IssueArticleCount">6</identifier><identifier type="VolumeIssueCount">3</identifier><part><date>1995</date><detail type="volume"><number>20</number><caption>vol.</caption></detail><detail type="issue"><number>1</number><caption>no.</caption></detail><extent unit="pages"><start>59</start><end>69</end></extent></part><recordInfo><recordOrigin>Kluwer Academic Publishers, 1995</recordOrigin></recordInfo></relatedItem><identifier type="istex">2B29DC7FF4A6B364AAAD2B85B2673778594C2E1E</identifier><identifier type="ark">ark:/67375/1BB-V549MB0T-P</identifier><identifier type="DOI">10.1007/BF01099918</identifier><identifier type="ArticleID">BF01099918</identifier><identifier type="ArticleID">Art4</identifier><accessCondition type="use and reproduction" contentType="copyright">Kluwer Academic Publishers, 1995</accessCondition><recordInfo><recordContentSource authority="ISTEX" authorityURI="https://loaded-corpus.data.istex.fr" valueURI="https://loaded-corpus.data.istex.fr/ark:/67375/XBH-3XSW68JL-F">springer</recordContentSource><recordOrigin>Kluwer Academic Publishers, 1995</recordOrigin></recordInfo></mods><json:item><extension>json</extension><original>false</original><mimetype>application/json</mimetype><uri>https://api.istex.fr/document/2B29DC7FF4A6B364AAAD2B85B2673778594C2E1E/metadata/json</uri></json:item></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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